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The Younger Dryas - National Climatic Data Center

NOAA National CENTERS FOR ENVIRONMENTAL INFORMATIONThe Younger DryasThe Younger Dryas is one of the most well-known examples of abrupt 14,500 years ago, Earth s climate began to shift from a cold glacial world to a warmer interglacial state. Partway through this transition, temperatures in the Northern Hemisphere suddenly returned to near-glacial conditions. This near-glacial period is called the Younger Dryas , named after a flower ( Dryas octopetala) that grows in cold conditions and that became common in Europe during this time. The end of the Younger Dryas , about 11,500 years ago, was par-ticularly abrupt. In Greenland, temperatures rose 10 C (18 F) in a decade (Alley 2000). Other proxy records, including varved lake sediments in Europe, also display these abrupt shifts (Brauer et al. 2008).The Younger Dryas is clearly observable in paleoclimate records from many parts of the world. In the Cariaco Basin north of Venezuela, for example, temperatures decreased about 3 C ( F), although some of this cooling might have been due to greater upwelling of colder subsurface water (Lea et al.)

in the Northern Hemisphere suddenly returned to near-glacial conditions. This near-glacial period is called the Younger Dryas, named after a flower (Dryas octopetala) that grows in cold conditions and that became common in Europe during this time. The end of the Younger Dryas, about 11,500 years ago, was par-ticularly abrupt.

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